简介:2015年5月-2016年4月,每月中旬纳潮前一天,现场观测辽宁旅顺口区江西镇大口井村面积3.33ha泥沙底海参Apostwhopusjaponicas池塘进、出水口表、底层溶解氧含量,并在夏(8月)、秋(11月)、冬(2月)和春季(4月)测定该池溶解氧含量的日昼夜垂直变。结果表明:冬季海参池塘溶解氧最高〉20mg/L,夏季最低至4.8mg/L;春、夏、秋表底层溶解氧含量不同,底层小于表层;表层高于底层,差值在1.5-4.0mg/L之间,夏季(8月)差值最大,达4.0mg/L。夏季池塘溶解氧含量昼夜及垂直变化幅度较大;冬季水层间溶解氧含量无昼夜变化。
简介:TheadsorptionkineticsofPb^2+ondifferentsoilsandmineralswithvariablechargeswasstudiedbythetwoion-selectiveelectrodetechniqueatdifferentpHandconcentrations.Theresultsshowedthatmorethan95%ofadsorptiononallthesamplesoccurredduringthefirst5minutes.Alladsorptiontime-dependentdatacouldfitthesurfacesecond-orderequationverywell.ThevaluesofXmweregoethite>kaolinite,andlatosol>redsoilatthesameinitialreactionconcentration.Thevaluesofkwerekaolinite>>goethite,andlatosol>redsoilatthesamereactionpHandinitialconcentration.ThehigherthesuspensionpH,thefastertheadsorptionoccurred.ThemeaningofXmgotbythetwoion-selectiveelectrodetechnique(onekindofbatchtechnique)wasdifferentfromthatbythemiscibledisplacementtechniqueinthattheformerwasonlytheequilibriumadsorptionamountatadefiniteconcentrationandpH,butthelatterwasalmostequaltotheadsorptioncapacityatadefinitepHwithmuchlessinfluenceofconcentration.OnePb^2+wassupposedtooccupytwoadsorptionsitesastheadsorptionmechanismisconcerned.